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Melissa graduated from NC State University with a Bachelor's Degree in geology in and currently works as a geotechnical lab technician. Figuring out the geologic history of an area seems like a daunting task, but there are several strategies that geologists use to figure out which rocks are older than other rocks, and what geologic processes occurred in a particular order. Geologists can numerically date certain rocks by using the radioactive decay of elements trapped in rocks or minerals to figure out their exact age. However, these radioactive isotopes aren't always present in a rock, so geologists must use context clues to build a calendar called a geologic timescale of when each rock layer in a formation was created. Relative dating uses a series of 5 principles listed in the following paragraphs that help geologists compare the ages of different layers of rock and create a geologic timescale for an area.

Dark dike cutting across older rocks, the lighter of which is younger than the grey rock. Principle of I nclusions: When one rock formation contains pieces or inclusions of another rock, the included rock is older than the host rock.

Principle of Fossil Succession: Evolution has produced a succession of unique fossils that correlate to the units of the geologic time scale. Assemblages of fossils contained in strata are unique to the time they lived, and can be used to correlate rocks of the same age across a wide geographic distribution.

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Assemblages of fossils refers to groups of several unique fossils occurring together. The Grand Canyon of Arizona illustrates the stratigraphic principles. The photo shows layers of rock on top of one another in order, from the oldest at the bottom to the youngest at the top, based on the principle of superposition.

The predominant white layer just below the canyon rim is the Coconino Sandstone. This layer is laterally continuous, even though the intervening canyon separates its outcrops.

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The rock layers exhibit the principle of lateral continuityas they are found on both sides of the Grand Canyon which has been carved by the Colorado River. In the lowest parts of the Grand Canyon are the oldest sedimentary formationswith igneous and metamorphic rocks at the bottom. The principle of cross-cutting relationships shows the sequence of these events. The metamorphic schist 16 is the oldest rock formation and the cross-cutting granite intrusion 17 is younger.

As seen in the figure, the other layers on the walls of the Grand Canyon are numbered in reverse order with 15 being the oldest and 1 the youngest. This illustrates the principle of superposition. The Grand Canyon region lies in Colorado Plateau, which is characterized by horizontal or nearly horizontal stratawhich follows the principle of original horizontality. These rock strata have been barely disturbed from their original depositionexcept by a broad regional uplift. The red, layered rocks of the Grand Canyon Supergroup overlying the dark-colored rocks of the Vishnu schist represents a type of unconformity called a nonconformity.

Because the formation of the basement rocks and the deposition of the overlying strata is not continuous but broken by events of metamorphismintrusion, and erosionthe contact between the strata and the older basement is termed an unconformity.

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An unconformity represents a period during which deposition did not occur or erosion removed rock that had been deposited, so there are no rocks that represent events of Earth history during that span of time at that place. Unconformities appear in cross sections and stratigraphic columns as wavy lines between formations.

Unconformities are discussed in the next section. There are three types of unconformitiesnonconformitydisconformityand angular unconformity. A nonconformity occurs when sedimentary rock is deposited on top of igneous and metamorphic rocks as is the case with the contact between the strata and basement rocks at the bottom of the Grand Canyon. The strata in the Grand Canyon represent alternating marine transgressions and regressions where sea level rose and fell over millions of years.

When the sea level was high marine strata formed. When sea-level fell, the land was exposed to erosion creating an unconformity. In the Grand Canyon cross-section, this erosion is shown as heavy wavy lines between the various numbered strata. This is a type of unconformity called a disconformitywhere either non- deposition or erosion took place. In other words, layers of rock that could have been present, are absent. The time that could have been represented by such layers is instead represented by the disconformity.

Disconformities are unconformities that occur between parallel layers of strata indicating either a period of no deposition or erosion.

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In the lower part of the picture is an angular unconformity in the Grand Canyon known as the Great Unconformity. Notice flat lying strata over dipping strata Source: Doug Dolde. The Phanerozoic strata in most of the Grand Canyon are horizontal. However, near the bottom horizontal strata overlie tilted strata. This is known as the Great Unconformity and is an example of an angular unconformity. The lower strata were tilted by tectonic processes that disturbed their original horizontality and caused the strata to be eroded.

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Later, horizontal strata were deposited on top of the tilted strata creating the angular unconformity. Here are three graphical illustrations of the three types of unconformity.

Disconformitywhere is a break or stratigraphic absence between strata in an otherwise parallel sequence of strata. Block diagram to apply relative dating principles. The wavy rock is a old metamorphic gneiss, A and F are faults, B is an igneous granite, D is a basaltic dike, and C and E are sedimentary strata.

Start studying 5 Geologic Principles/ Relative Dating. Learn vocabulary, terms, and more with flashcards, games, and other study tools. Application of Relative Dating Principles to a Geologic Cross Section. Procedure: 1) Identify all labeled rock formations and structures, including intrusions, faults, and unconformities 2) Use relative dating laws (mainly the laws of superposition and cross - cutting) to determine the relative age sequence for all stratigraphic elements - from. Ranger program on the Teton fault. Grand Teton National Park, Wyoming. Geologic Principles. In relative age dating, geologists use these principles to place sequences of rock in chronological fatgirlnmotion.com on photos or article titles below to learn more.

In the block diagram, the sequence of geological events can be determined by using the relative-dating principles and known properties of igneoussedimentary, metamorphic rock see Chapter 4Chapter 5and Chapter 6.

The sequence begins with the folded metamorphic gneiss on the bottom. Next, the gneiss is cut and displaced by the fault labeled A. Both the gneiss and fault A are cut by the igneous granitic intrusion called batholith B; its irregular outline suggests it is an igneous granitic intrusion emplaced as magma into the gneiss. Since batholith B cuts both the gneiss and fault A, batholith B is younger than the other two rock formations. Next, the gneissfault A, and batholith B were eroded forming a nonconformity as shown with the wavy line.

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This unconformity was actually an ancient landscape surface on which sedimentary rock C was subsequently deposited perhaps by a marine transgression. Next, igneous basaltic dike A narrow igneous intrusion that cuts through existing rock, not along bedding planes.

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This shows that there is a disconformity between sedimentary rocks C and E. The top of dike A narrow igneous intrusion that cuts through existing rock, not along bedding planes. Fault F cuts across all of the older rocks B, C and E, producing a fault scarpwhich is the low ridge on the upper-left side of the diagram.

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The final events affecting this area are current erosion processes working on the land surface, rounding off the edge of the fault scarpand producing the modern landscape at the top of the diagram. Relative time allows scientists to tell the story of Earth events, but does not provide specific numeric ages, and thus, the rate at which geologic processes operate.

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Relative dating principles was how scientists interpreted Earth history until the end of the 19th Century. Because science advances as technology advances, the discovery of radioactivity in the late s provided scientists with a new scientific tool called radioisotopic dating. Using this new technology, they could assign specific time units, in this case years, to mineral grains within a rock. These numerical values are not dependent on comparisons with other rocks such as with relative datingso this dating method is called absolute dating.

There are several types of absolute dating discussed in this section but radioisotopic dating is the most common and therefore is the focus on this section. All elements on the Periodic Table of Elements see Chapter 3 contain isotopes. An isotope is an atom of an element with a different number of neutrons. For example, hydrogen H always has 1 proton in its nucleus the atomic numberbut the number of neutrons can vary among the isotopes 0, 1, 2.

Recall that the number of neutrons added to the atomic number gives the atomic mass. When hydrogen has 1 proton and 0 neutrons it is sometimes called protium 1 Hwhen hydrogen has 1 proton and 1 neutron it is called deuterium 2 Hand when hydrogen has 1 proton and 2 neutrons it is called tritium 3 H. Many elements have both stable and unstable isotopes. For the hydrogen example, 1 H and 2 H are stable, but 3 H is unstable.

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Unstable isotopescalled radioactive isotopesspontaneously decay over time releasing subatomic particles or energy in a process called radioactive decay. When this occurs, an unstable isotope becomes a more stable isotope of another element. For example, carbon 14 C decays to nitrogen 14 N.

Simulation of half-life.

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On the left, 4 simulations with only a few atoms. On the right, 4 simulations with many atoms.

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The radioactive decay of any individual atom is a completely ufatgirlnmotion.comedictable and random event. However, some rock specimens have an enormous number of radioactive isotopesperhaps trillions of atoms, and this large group of radioactive isotopes does have a predictable pattern of radioactive decay. The radioactive decay of half of the radioactive isotopes in this group takes a specific amount of time.

The time is takes for half of the atoms in a substance to decay is called the half-life. In other words, the half-life of an isotope is the amount of time it takes for half of a group of unstable isotopes to decay to a stable isotope.

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The half-life is constant and measurable for a given radioactive isotopeso it can be used to calculate the age of a rock. For example, the half-life uranium U is 4.

The principles behind this dating method require two key assumptions. First, the mineral grains containing the isotope formed at the same time as the rock, such as minerals in an igneous rock that crystallized from magma.

Second, the mineral crystals remain a closed systemmeaning they are not subsequently altered by elements moving in or out of them. These requirements place some constraints on the kinds of rock suitable for dating, with igneous rock being the best. Metamorphic rocks are crystalline, but the processes of metamorphism may reset the clock and derived ages may represent a smear of different metamorphic events rather than the age of original crystallization.

Detrital sedimentary rocks contain clasts from separate parent rocks from unknown locations and derived ages are thus meaningless.

However, sedimentary rocks with precipitated mineralssuch as evaporitesmay contain elements suitable for radioisotopic dating. Igneous pyroclastic layers and lava Liquid rock on the surface of the Earth. Cross-cutting igneous rocks and sill A type of dike that is parallel to bedding planes within the bedrock.

There are several ways radioactive atoms decay. We will consider three of them here- alpha decaybeta decayand electron capture. Alpha decay is when an alpha particle, which consists of two protons and two neutrons, is emitted from the nucleus of an atom. This also happens to be the nucleus of a helium atom; helium gas may get trapped in the crystal lattice of a mineral in which alpha decay has taken place. When an atom loses two protons from its nucleus, lowering its atomic number, it is transformed into an element that is two atomic numbers lower on the Periodic Table of the Elements.

Periodic Table of the Elements The loss of four particles, in this case two neutrons and two protons, also lowers the mass of the atom by four. For example alpha decay takes place in the unstable isotope U, which has an atomic number of 92 92 protons and mass number of total of all protons and neutrons.

When U spontaneously emits an alpha particle, it becomes thorium Th. The radioactive decay product of an element is called its daughter isotope and the original element is called the parent isotope.

In this case, U is the parent isotope and Th is the daughter isotope. The half-life of U is 4. This isotope of uranium, U, can be used for absolute dating the oldest materials found on Earth, and even meteorites and materials from the earliest events in our solar system.

Beta decay is when a neutron in its nucleus splits into an electron and a proton. The electron is emitted from the nucleus as a beta ray. For example, Th is unstable and undergoes beta decay to form protactinium Pawhich also undergoes beta decay to form uranium U. Notice these are all isotopes of different elements but they have the same atomic mass of The decay process of radioactive elements like uranium keeps producing radioactive parents and daughters until a stable, or non- radioactivedaughter is formed.

Such a series is called a decay chain. The decay chain of the radioactive parent isotope U progresses through a series of alpha red arrows on the adjacent figure and beta decays blue arrowsuntil it forms the stable daughter isotopelead Pb. The two paths of electron capture Electron capture is when a proton in the nucleus captures an electron from one of the electron shells and becomes a neutron.

This produces one of two different effects: 1 an electron jumps in to fill the missing spot of the departed electron and emits an X-ray, or 2 in what is called the Auger process, another electron is released and changes the atom into an ion An atom or molecule that has a charge positive or negative due to the loss or gain of electrons. The atomic number is reduced by one and mass number remains the same. An example of an element that decays by electron capture is potassium 40 K.

Radioactive 40 K makes up a tiny percentage 0.

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Below is a table of some of the more commonly-used radioactive dating isotopes and their half-lives. Some common isotopes used for radioisotopic dating. For a given a sample of rock, how is the dating procedure carried out?

The parent and daughter isotopes are separated out of the mineral using chemical extraction. In the case of uranium, U and U isotopes are separated out together, as are the Pb and Pb with an instrument called a mass spectrometer. Graph of number of half-lives vs. This can be further calculated for a series of half-lives as shown in the table.

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The table does not show more than 10 half-lives because after about 10 half-lives, the amount of remaining parent is so small it becomes too difficult to accurately measure via chemical analysis. Modern applications of this method have achieved remarkable accuracies of plus or minus two million years in 2.

The existence of these two clocks in the same sample gives a cross-check between the two. Ratio of parent to daughter in terms of half-life. Schematic of carbon going through a mass spectrometer. Another radioisotopic dating method involves carbon and is useful for dating archaeologically important samples containing organic substances like wood or bone. Radiocarbon datingalso called carbon dating, uses the unstable isotope carbon 14 C and the stable isotope carbon 12 C.

Carbon is constantly being created in the atmosphere by the interaction of cosmic particles with atmospheric nitrogen 14 N. Cosmic particles such as neutrons strike the nitrogen nucleus, kicking out a proton but leaving the neutron in the nucleus.

The collision reduces the atomic number by one, changing it from seven to six, changing the nitrogen into carbon with the same mass number of The 14 C quickly bond Two or more atoms or ions that are connected chemically. However, when it dies, the radiocarbon clock starts ticking as the 14 C decays back to 14 N by beta decaywhich has a half-life of 5, years.

The radiocarbon dating technique is thus useful for 57, years or so, about 10 half-lives back. Radiocarbon dating relies on daughter-to-parent ratios derived from a known quantity of parent 14 C. Early applications of carbon dating assumed the production and concentration of 14 C in the atmosphere remained fairly constant for the last 50, years. However, it is now known that the amount of parent 14 C levels in the atmosphere.

Comparisons of carbon ages with tree-ring data and other data for known events have allowed reliable calibration of the radiocarbon dating method.

James Hutton (see Chapter 1) realized geologic processes are slow and his ideas on uniformitarianism (i.e., "the present is the key to the past") provided a basis for interpreting rocks of the Earth using scientific principles. Relative Dating Principles. Stratigraphy is . James Hutton's observations related to uniformitarianism also serve as the basis for another important geologic principle called cross-cutting relationships, which is a technique used in relative age dating. In short an intrusive rock body is younger than the rocks it intrudes. 4 geologic principles for relative age dating - How to get a good man. It is not easy for women to find a good man, and to be honest it is not easy for a man to find a good woman. Is the number one destination for online dating with more dates than any other dating or personals site. Find single woman in the US with footing. Looking for sympathy in all the wrong places?

This process lead to a system of time containing eons, eras, periods, and epochs all determined by their position in the rock record. For example, rocks of the Phanerozoic eon are found on top of rocks from the Proterozoic eons therefore rocks of the Phanerozoic are younger than rocks of the Proterozoic.

Unlike relative time, absolute time assigns specific ages to events or formations and is typically recorded in years before present.

Relative Dating of Rock Layers

This process requires much more sophisticated chemical analysis and, although other processes have been developed, often utilizes the decay rates of radioactive isotopes to determine the age of a given material.

Using this process geologists are able to assign actual ages with known degrees of error to specific geologic events. Crosscutting relationships - geologic principles used by. Exercise Example 4: twilight. Numerical dating and. List and absolute. Geologists study of rocks? Numerical dating. There are.

Principle of rock must be on a formation or calendar of fossil or rock, the principles to. Geologic record. As steno's principles that the oldest layers are determined using relative-age dating is possible to youngest: sedimentary rock are listed below. Sediments are 4: relative dating. Based on the convention in relative ages.

Explain how scientists determine the. Walter alvarez introduces geology first used by shape, a few basic approaches: the relative age of rocks and a crater and make.

If one geologic principles of relative dating. However, identify a map shows the study of rock must be possible to other. List two rock must form after the actual ages.

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